ch. 4- rocks

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Ch. 4- Rocks

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Ch. 4- Rocks . Rock : solid mixture of crystals of 1 or more minerals. Characteristics to Classify Rocks . Composition : minerals that make up rock Texture : size, shape, and positions of the grains in rock 1. Fine grained 2. Medium grained 3. Coarse grained. Rock Cycle . - PowerPoint PPT Presentation

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Page 1: Ch. 4- Rocks

Ch. 4- Rocks

Page 2: Ch. 4- Rocks

• Rock: solid mixture of crystals of 1 or more minerals.

Page 3: Ch. 4- Rocks

Characteristics to Classify Rocks

• Composition: minerals that make up rock

• Texture: size, shape, and positions of the grains in rock

• 1. Fine grained• 2. Medium grained• 3. Coarse grained

Page 4: Ch. 4- Rocks

Rock Cycle • Rock cycle is a continual process

by which new rock form from old rock material.

Page 5: Ch. 4- Rocks

• Processes that shape the surface of the earth: –Weathering– Erosion–Deposition– Uplift

Page 6: Ch. 4- Rocks

Sedimentary Rock• Form by process of erosion and

weathering to break down other rocks into sediment which is deposited and compacted

Page 7: Ch. 4- Rocks

Sedimentary Rock• 3 types of sedimentary rock: – 1. Clastic Sedimentary rock- forms

when rock or mineral fragments are cemented together • Classified by size of fragments they are

made of – 2. Chemical Sedimentary rock: form

from solutions of dissolved minerals and water• Crystallize out of solutions- EX- salt

water

Page 8: Ch. 4- Rocks

– 3. Organic- forms from remains of plants and animals that cement together• EX- limestone

• Sedimentary structures include:– Ripple marks–Mud cracks– Raindrop impressions

Page 9: Ch. 4- Rocks

Metamorphic Rock• “meta”= change• “morphos”= shape

• Structure, texture, or composition has changed.

• Most common metamorphic change is caused by pressure

Page 10: Ch. 4- Rocks

Texture of Metamorphic Rock

• Foliated metamorphic rocks- mineral crystals aligned in planes or bands

• Non-foliated metamorphic rocks- not aligned crystals

• Metamorphic structures are caused by deformation.

Page 11: Ch. 4- Rocks

2 Types of Metamorphism

• 1. Contact Metamorphism: when a rock comes on contact w/ magma or heat from magma.–Only occurs next to igneous

intrusions• 2. Regional Metamorphism:

enormous pressure b/w deeply buried rock or when crusts collide causing heat and the pressure to change rock.

Page 12: Ch. 4- Rocks

Igneous Rock• Igneous comes from the Latin

word “fire”• Form when magma cools and

hardens• Texture is determined by rate at

which the rock cools

Page 13: Ch. 4- Rocks

• Igneous rock that solidifies at Earth’s surface- extrusive

• Igneous rock that solidifies within earth’s surface- intrusive

Page 14: Ch. 4- Rocks

• Common shapes of intrusive igneous bodies: – Batholiths– Stocks– Sills–Dikes

Page 15: Ch. 4- Rocks

• Classifying Igneous Rock:• 1. Felsic:– Light colored– Less dense– Rich in silicon, aluminum, sodium,

potassium• 2. Mafic:–Dark colored–More dense– Rich in iron, magnesium, calcium